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The Kelvin-Helmholtz to Holmboe instability transition in stratified exhange flows

The Kelvin-Helmholtz to Holmboe instability transition in stratified exhange flows
The Kelvin-Helmholtz to Holmboe instability transition in stratified exhange flows
A laboratory investigation of exchange flows near the two-layer hydraulic limit is used to examine the generation of shear instability at the interface dividing the two layers. The present experiments differ from many previous investigations into shear instability, in that the instabilities are an active part of a quasi-steady flow regime rather than the product of a controlled initial state. Regimes characterized by either Kelvin–Helmholtz or Holmboe's instability are found to be separated by a well-defined transition. Observations of the transition from Kelvin–Helmholtz to Holmboe's instability are compared to predictions from scaling arguments that draw on elements of both two-layer hydraulic theory and linear stability theory. The characteristics of unstable modes near the transition, and the structure of both classes of instability are examined in detail.
KELVIN HELMHOLTZ INSTABILITY, STRATIFIED FLOW
0022-1120
339-362
Hogg, A.M.
df48090a-bbe6-4929-a94a-62a0aa7e5e8b
Ivey, G.N.
4159aad2-428c-4c58-b1cb-201d50928b3a
Hogg, A.M.
df48090a-bbe6-4929-a94a-62a0aa7e5e8b
Ivey, G.N.
4159aad2-428c-4c58-b1cb-201d50928b3a

Hogg, A.M. and Ivey, G.N. (2003) The Kelvin-Helmholtz to Holmboe instability transition in stratified exhange flows. Journal of Fluid Mechanics, 477, 339-362. (doi:10.1017/S0022112002003397).

Record type: Article

Abstract

A laboratory investigation of exchange flows near the two-layer hydraulic limit is used to examine the generation of shear instability at the interface dividing the two layers. The present experiments differ from many previous investigations into shear instability, in that the instabilities are an active part of a quasi-steady flow regime rather than the product of a controlled initial state. Regimes characterized by either Kelvin–Helmholtz or Holmboe's instability are found to be separated by a well-defined transition. Observations of the transition from Kelvin–Helmholtz to Holmboe's instability are compared to predictions from scaling arguments that draw on elements of both two-layer hydraulic theory and linear stability theory. The characteristics of unstable modes near the transition, and the structure of both classes of instability are examined in detail.

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Published date: 2003
Keywords: KELVIN HELMHOLTZ INSTABILITY, STRATIFIED FLOW

Identifiers

Local EPrints ID: 2104
URI: http://eprints.soton.ac.uk/id/eprint/2104
ISSN: 0022-1120
PURE UUID: aa1f7cc0-3036-4c20-9b70-1a294a23e25d

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Date deposited: 11 May 2004
Last modified: 15 Mar 2024 04:44

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Contributors

Author: A.M. Hogg
Author: G.N. Ivey

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